Stable isotope data and sedimentary major element concentration of sediment c...
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Negative stable carbon isotopic excursions have been observed throughout most of the mid-depth (~1000-3000m) Atlantic Ocean during Heinrich Stadial 1 (HS1) and the Younger Dryas...
在海因里希冷期1(Heinrich Stadial 1,HS1)与新仙女木期(Younger Dryas)期间,大西洋绝大多数中层海域(水深约1000~3000米)均观测到稳定碳同位素负偏现象



